PepinPlamondonStein1992

Référence

Pepin, S., Plamondon, A.P., Stein, J. (1992) Peat water-content measurement using time domain reflectometry. Canadian Journal of Forest Research, 22(4):534-540.

Résumé

The calibration of time domain reflectometry, previously established for an organic soil of 0.422 Mg.m-3 bulk density, was established for peat blocks with bulk densities ranging from 0.06 to 0.25 Mg.m-3. An empirical relationship between the volumetric water content and the measured apparent dielectric constant was established in the laboratory. This relationship can be used to estimate volumetric water content between 0.21 and 0.95 cm3.cm-3 with a standard deviation of 0.03 cm3.cm-3. The large variations observed during the calibration were mainly attributed to the size and heterogeneousness of peat samples. When water tables in the field were high, standard deviation decreased to 0.02 cm3.cm-3, which agrees very well with other time domain reflectometry experiments.

Format EndNote

Vous pouvez importer cette référence dans EndNote.

Format BibTeX-CSV

Vous pouvez importer cette référence en format BibTeX-CSV.

Format BibTeX

Vous pouvez copier l'entrée BibTeX de cette référence ci-bas, ou l'importer directement dans un logiciel tel que JabRef .

@ARTICLE { PepinPlamondonStein1992,
    AUTHOR = { Pepin, S. and Plamondon, A.P. and Stein, J. },
    TITLE = { Peat water-content measurement using time domain reflectometry },
    JOURNAL = { Canadian Journal of Forest Research },
    YEAR = { 1992 },
    VOLUME = { 22 },
    PAGES = { 534-540 },
    NUMBER = { 4 },
    ABSTRACT = { The calibration of time domain reflectometry, previously established for an organic soil of 0.422 Mg.m-3 bulk density, was established for peat blocks with bulk densities ranging from 0.06 to 0.25 Mg.m-3. An empirical relationship between the volumetric water content and the measured apparent dielectric constant was established in the laboratory. This relationship can be used to estimate volumetric water content between 0.21 and 0.95 cm3.cm-3 with a standard deviation of 0.03 cm3.cm-3. The large variations observed during the calibration were mainly attributed to the size and heterogeneousness of peat samples. When water tables in the field were high, standard deviation decreased to 0.02 cm3.cm-3, which agrees very well with other time domain reflectometry experiments. },
    KEYWORDS = { ELECTROMAGNETIC DETERMINATION; TRANSMISSION-LINES; SOIL; TDR },
    OWNER = { brugerolles },
    TIMESTAMP = { 2007.12.05 },
}

********************************************************** ***************** Facebook Twitter *********************** **********************************************************

Abonnez-vous à
l'Infolettre du CEF!

********************************************************** ***************** Pub - Mycorhizes_2019 ****************** **********************************************************

********************************************************** ***************** Pub - Symphonies_Boreales ****************** **********************************************************

********************************************************** ***************** Boîte à trucs *************** **********************************************************

CEF-Référence
La référence vedette !

Jérémie Alluard (2016) Les statistiques au moments de la rédaction 

  • Ce document a pour but de guider les étudiants à intégrer de manière appropriée une analyse statistique dans leur rapport de recherche.

Voir les autres...